( 303 > 
^Hts . 
!>3m *iver 
‘ of 
TBE TREKT. 
t ' Of o. among the moor-lands in the north-wesl 
fj j °>'dshire, and having received the tribute of 
lO*'Bs streams, runs to tlie eastward. It 
H?* shifg “^'igable at Burton-upon-Trent, where it leaves 
flowing through Derbphire, Nottingham, 
^'ncolnshire, discharges itself into tliat great 
of northern rivers, the Humber, after a 
hundred miles. It enters Notting- 
't '^"'As south-west point, and being tliere joined by 
it passes to the eastward till it reaches Newark, 
% ® island; when, turning to the nortli, 
•vlj^aty p about fourteen miles, it constitutes tlie 
'ivt ® Tip fl'ife on the side of Lincolnshire. 
itsil tiov J'*' '* j°ined a little below Burton by the beautiful 

V ■ ‘ • 
'Op \ 
>ow. 
■'vhichj rising at the most northern point of 
if’ the boundary between it and Derby- 
'tJi’ thg the Trent a little below Burton, 
p'"". rises a few miles 
Another 
to the west of New- 
on the south-east, 
in Derbyshire, 
the northern part of Nottingham- 
ac a little distance 
In its course a subterraiieous tunnel 
Csk “Qer I- u .v.« iiiiu.., ii. 11 
has V”*^’ and falls into the Trent m 
*S *’ Passi formed from Chesteifield, 
'^e*iUn,''®.’'^“'ough the northern i 
^ L ^ain,K 'with the Trent 
exte Norwood hill, upwards ot a mile and 
n-.. . > and so straight, that the termination at 
IS-. straight, 
®®en at the other. 
r, IIL ixie Ol 
I three inches 
that the termination at 
l ire itreh is twelve feet 
ttnd 7“^'^ "uenes in width, and in the deepest 
beneath the surface of the 
Jtiii a, g ® rimnerous canals formed in the north of 
’**'tr.^*’d . 1 , °?iriunication is now oitened between the 
Wes/tte Me 
I 
''tst, ■‘■''lersey, or' quite across tlie kingdom, from 
&*"> 
» Eill 
THE HUMIiEIl. 
into the Humber arc the Ouse, oi 
Vlus ^ ■“‘P’ '"e -HU..11S11K ine me v^uoc, oi 
111 Mhp those by which the Ouse itself is 
th <2 Derwent, the Calder, 
Nidd, the Vote, and the Swale. 
side of Yorkshai^ 
^ 'a the west-north-west 
ft 2 
